在西藏高原,放牧逆转了气候引起的土壤碳增加
Shuai Ren1, Tao Wang2, Xinhui Ji1,3
1State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China.
Nature communications
|July 29, 2025
概括
西藏高原的土壤将因变暖而增加碳,但大部分是脆弱的. 优化畜牧放牧对于保持这些土壤碳汇对抗气候变化影响至关重要.
科学领域:
- 环境科学 环境科学
- 土壤科学 土壤科学
- 气候科学 气候科学
背景情况:
- 西藏高原的土壤碳库存面临气候变暖和牲畜放牧增加的威胁.
- 目前对这些影响的模型预测是不受限制的,缺乏确定性.
研究的目的:
- 预测气候变化和放牧对土壤碳库存的影响,使用综合数据和三池模型.
- 评估土壤碳增加对极端事件和放牧压力的脆弱性.
主要方法:
- 整合大规模的土壤采样活动和土壤化实验.
- 配对放牧实验以模拟不同的牲畜管理场景.
- 应用三池土壤碳模型用于预测.
主要成果:
- 预计西藏土壤将充当碳汇,但超过一半的碳增量是在活跃的,脆弱的池中.
- 即使在平衡状态下,继续放牧可能会抵消气候引起的碳捕集效益.
- 热岩过程不太可能扭转整体趋势,但有助于碳动态.
结论:
- 优化牧场管理对于维持西藏高原的土壤碳汇至关重要.
- 纳入放牧对土壤碳的影响对于改进地球系统模型至关重要.
- 活性土壤碳池的脆弱性需要西藏高原的适应性管理策略.
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